Jr. Olson et al., THERMAL-CONDUCTIVITY OF DIAMOND BETWEEN 170 AND 1200-K AND THE ISOTOPE EFFECT, Physical review. B, Condensed matter, 47(22), 1993, pp. 14850-14856
Measurements on the thermal conductivity of natural and synthetic sing
le-crystal diamond are presented over a wide temperature range. The la
rge isotope effect reported previously has been confirmed. The data ha
ve been analyzed using both the Debye model of thermal conductivity, w
hich ignores the N processes, and the Callaway model in the limit that
the N processes dominate the phonon scattering. It is found that the
observed isotope effect can be accounted for by including the N proces
ses alone, without having to postulate the existence of additional def
ects.